Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Liangtian Ni"'
Publikováno v:
Journal of Petroleum Science and Technology, Vol 5, Iss 1, Pp 28-39 (2015)
This study aims to identify favorable oil–gas reservoir facies in the Chishan group of the Wubao fault zone (Gaoyou sag, Subei basin, China) using the methods of outcrops and cores observation, granularity analysis, scanning electron microscope, lo
Externí odkaz:
https://doaj.org/article/c84e2e7563bc4b068b167b5e975979c9
Ordovician carbonate rock matrix fractured-porous reservoirs in Tahe Oilfield, Tarim Basin, NW China
Publikováno v:
Petroleum Exploration and Development, Vol 41, Iss 6, Pp 745-753 (2014)
Features of porphyritic limestone matrix fracture-vug reservoirs in Tahe Oilfield, Tarim Basin, NW China was examined by core observation, thin section identification, cathodoluminescence, microscopic fluorescence, scanning electron microscope and en
Externí odkaz:
https://doaj.org/article/8e68fd98f18e48f3a676834153486788
Publikováno v:
Journal of Earth Science. 26:677-689
A particular type of soft-sediment deformation structure, similar to imbricate structure, is developed in the Jurassic strata at Honggouzi, western Qaidam Basin, China. We refer to this structure as a duplex-like deformation structure, because it is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9cbe6702f92d90d0ac05501a6abe76e0
https://doi.org/10.1007/s12583-015-0578-2
https://doi.org/10.1007/s12583-015-0578-2
Ordovician carbonate rock matrix fractured-porous reservoirs in Tahe Oilfield, Tarim Basin, NW China
Publikováno v:
Petroleum Exploration and Development, Vol 41, Iss 6, Pp 745-753 (2014)
Features of porphyritic limestone matrix fracture-vug reservoirs in Tahe Oilfield, Tarim Basin, NW China was examined by core observation, thin section identification, cathodoluminescence, microscopic fluorescence, scanning electron microscope and en
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::71e835ee4eab28bf41ae2e5b35b89e70
https://doi.org/10.1016/s1876-3804(14)60088-4
https://doi.org/10.1016/s1876-3804(14)60088-4
Autor:
WeiHua Li, Yuan Tian, XiaoNan Wang, XinYing Cui, YunTian Liu, Cui Mao, Shengxin Liu, Jianhua Zhong, Gangshan Lin, Liangtian Ni, Zhufu Shao, Yong Li
Publikováno v:
Science China Earth Sciences. 57:1061-1076
Imbricate structure is a common sedimentary structure and is well developed in sandy sediments. Here, we report a lamina-controlled fine-sand-particle imbricate structure in a set of very fine grained sedimentary rocks (fine sandstone, siltstone, and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6537efa7eb144c94e78cbb9092a16ab7
https://doi.org/10.1007/s11430-014-4848-x
https://doi.org/10.1007/s11430-014-4848-x
Autor:
Jianhua, Zhong1, Liangtian, Ni1, Ningliang, Sun1, Chuang, Liu1, Bing, Hao1, Mengchun, Cao1, xin, Chen1, Ke, Luo1, Shengxin, Liu1, Leitong, Huang1, Guanqun, Yang1, Shaojie, Wang1, Feifei, Su1, Xuejing, He1, Yanqiu, Xue1
Publikováno v:
Scientific Reports. 11/11/2016, p36945. 1p.